WEKO3
アイテム
{"_buckets": {"deposit": "aa5fa8b9-af48-471d-98ba-20a33770f0c3"}, "_deposit": {"created_by": 3, "id": "392", "owners": [3], "pid": {"revision_id": 0, "type": "depid", "value": "392"}, "status": "published"}, "_oai": {"id": "oai:shizuoka.repo.nii.ac.jp:00000392", "sets": ["107"]}, "author_link": ["219", "320", "321"], "item_25_biblio_info_5": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1994-03", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "142", "bibliographicPageStart": "135", "bibliographicVolumeNumber": "20", "bibliographic_titles": [{"bibliographic_title": "Geoscience reports of Shizuoka University"}]}]}, "item_25_description_2": {"attribute_name": "資源タイプ", "attribute_value_mlt": [{"subitem_description": "Departmental Bulletin Paper", "subitem_description_type": "Other"}]}, "item_25_description_30": {"attribute_name": "フォーマット", "attribute_value_mlt": [{"subitem_description": "application/pdf", "subitem_description_type": "Other"}]}, "item_25_description_9": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "The Waitemata Group in the Upper Waitemata Harbour area is a turbidite sequence with interbedded volcaniclastic sandstones, rhyolitic granule-sand and tuff horizons, and conglomerate lenses containing metamorphic, volcanic, plutonic and sedimentary clasts. Clastic debris in the sediments is little altered except for devitrification of volcanic glass. Zeolites and clay minerals encrust clastic grains and fill pores. There is a strong lithologic control on diagenetic assemblages. Lithic-rich sandstones poor in volcanic debris have calcite cement. Volcaniclastic sandstones have zeolite cement with the paragenetic sequence clinoptilolite ( + mordenite) → chabazite and/or erionite, and finally rare analcime. Rhyolitic granule-sand horizons contain the paragenetic sequence analcime → clinoptilolite → chabazite and/or erionite. Conglomerate horizons, which frequently lack any vitric debris, have analcime cement. In rhyolitic tuff only mordenite occurs crystallising directly from devitrified glass shards. Clay minerals present are smectite and illite, and chlorite in highly altered volcaniclastic sediments. Interbedded mudstones sealed fluids into volcaniclastic sandstone and tuff horizons and diagenesis occurred in a closed hydrologic system. The original pore fluid, believed bicarbonate-rich, precipitated calcite cement in the absence of vitric debris. In volcaniclastic and vitric rocks devitrification of glass liberated alkalies and silica into pore fluids leading to crystallisation of zeolite. Conglomerates filling channels cut into other sediments were an open hydrologic system and analcime crystallised from Na-saturated fluids flowing through them.", "subitem_description_type": "Abstract"}]}, "item_25_full_name_3": {"attribute_name": "提供者", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "219", "nameIdentifierScheme": "WEKO"}, {"nameIdentifier": "219", "nameIdentifierScheme": "wekoID", "nameIdentifierURI": "https://shizuoka.repo.nii.ac.jp/?action=pages_view_main\u0026active_action=repository_view_main_item_snippet\u0026meta=\u0026wekoAuthorId=219\u0026count=20\u0026order=16\u0026pn=1\u0026page_id=13\u0026block_id=21"}, {"nameIdentifier": "a312ddb6-239f-4b32-b9b7-e512370e7d62", "nameIdentifierScheme": "著者リンク", "nameIdentifierURI": "http://uni.lib.shizuoka.ac.jp/Record/a312ddb6-239f-4b32-b9b7-e512370e7d62"}], "names": [{"name": "(DUMMY)[学外・非常勤講師]"}]}]}, "item_25_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.14945/00000312", "subitem_identifier_reg_type": "JaLC"}]}, "item_25_publisher_6": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "Shizuoka University. Institute of Geosciences"}]}, "item_25_relation_22": {"attribute_name": "NII論文ID", "attribute_value_mlt": [{"subitem_relation_type": "isIdenticalTo", "subitem_relation_type_id": {"subitem_relation_type_id_text": "110000413352", "subitem_relation_type_select": "NAID"}}]}, "item_25_source_id_19": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "03886298", "subitem_source_identifier_type": "ISSN"}]}, "item_25_source_id_23": {"attribute_name": "NII書誌ID", "attribute_value_mlt": [{"subitem_source_identifier": "AN00103190", "subitem_source_identifier_type": "NCID"}]}, "item_25_subject_8": {"attribute_name": "NDC", "attribute_value_mlt": [{"subitem_subject": "458", "subitem_subject_scheme": "NDC"}]}, "item_25_version_type_32": {"attribute_name": "著者版フラグ", "attribute_value_mlt": [{"subitem_version_resource": "http://purl.org/coar/version/c_970fb48d4fbd8a85", "subitem_version_type": "VoR"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Davidson, Kevin J."}], "nameIdentifiers": [{"nameIdentifier": "320", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Black, Philippa M."}], "nameIdentifiers": [{"nameIdentifier": "321", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2017-12-14"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00000102365.pdf", "filesize": [{"value": "1.5 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 1500000.0, "url": {"label": "KJ00000102365.pdf", "url": "https://shizuoka.repo.nii.ac.jp/record/392/files/KJ00000102365.pdf"}, "version_id": "73a3e75e-a0e7-4fd1-bf64-9841acd5276f"}]}, "item_keyword": {"attribute_name": "キーワード", "attribute_value_mlt": [{"subitem_subject": "zeolites", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}, {"subitem_subject": "analcime", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}, {"subitem_subject": "New Zealand", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}, {"subitem_subject": "rhyolitic tuffs", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}, {"subitem_subject": "volcaniclastic sediments", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Waitemata Group", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_resource_type": {"attribute_name": "資源タイプ", "attribute_value_mlt": [{"resourcetype": "departmental bulletin paper", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "Diagenesis in Early Miocene Waitemata Group sediments, Upper Waitemata Harbour, Auckland, New Zealand(MEMORIAL VOLUME TO THE LATE PROFESSOR TERUHIKO SAMESHIMA)", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Diagenesis in Early Miocene Waitemata Group sediments, Upper Waitemata Harbour, Auckland, New Zealand(MEMORIAL VOLUME TO THE LATE PROFESSOR TERUHIKO SAMESHIMA)", "subitem_title_language": "en"}]}, "item_type_id": "25", "owner": "3", "path": ["107"], "permalink_uri": "https://doi.org/10.14945/00000312", "pubdate": {"attribute_name": "公開日", "attribute_value": "2008-01-25"}, "publish_date": "2008-01-25", "publish_status": "0", "recid": "392", "relation": {}, "relation_version_is_last": true, "title": ["Diagenesis in Early Miocene Waitemata Group sediments, Upper Waitemata Harbour, Auckland, New Zealand(MEMORIAL VOLUME TO THE LATE PROFESSOR TERUHIKO SAMESHIMA)"], "weko_shared_id": 3}
Diagenesis in Early Miocene Waitemata Group sediments, Upper Waitemata Harbour, Auckland, New Zealand(MEMORIAL VOLUME TO THE LATE PROFESSOR TERUHIKO SAMESHIMA)
https://doi.org/10.14945/00000312
https://doi.org/10.14945/00000312d0402659-7481-4813-a311-2a74f7a03954
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000102365.pdf (1.5 MB)
|
|
Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2008-01-25 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Diagenesis in Early Miocene Waitemata Group sediments, Upper Waitemata Harbour, Auckland, New Zealand(MEMORIAL VOLUME TO THE LATE PROFESSOR TERUHIKO SAMESHIMA) | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | zeolites | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | analcime | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | New Zealand | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | rhyolitic tuffs | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | volcaniclastic sediments | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Waitemata Group | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.14945/00000312 | |||||
ID登録タイプ | JaLC | |||||
著者 |
Davidson, Kevin J.
× Davidson, Kevin J.× Black, Philippa M. |
|||||
書誌情報 |
Geoscience reports of Shizuoka University 巻 20, p. 135-142, 発行日 1994-03 |
|||||
出版者 | ||||||
出版者 | Shizuoka University. Institute of Geosciences | |||||
NDC | ||||||
主題Scheme | NDC | |||||
主題 | 458 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The Waitemata Group in the Upper Waitemata Harbour area is a turbidite sequence with interbedded volcaniclastic sandstones, rhyolitic granule-sand and tuff horizons, and conglomerate lenses containing metamorphic, volcanic, plutonic and sedimentary clasts. Clastic debris in the sediments is little altered except for devitrification of volcanic glass. Zeolites and clay minerals encrust clastic grains and fill pores. There is a strong lithologic control on diagenetic assemblages. Lithic-rich sandstones poor in volcanic debris have calcite cement. Volcaniclastic sandstones have zeolite cement with the paragenetic sequence clinoptilolite ( + mordenite) → chabazite and/or erionite, and finally rare analcime. Rhyolitic granule-sand horizons contain the paragenetic sequence analcime → clinoptilolite → chabazite and/or erionite. Conglomerate horizons, which frequently lack any vitric debris, have analcime cement. In rhyolitic tuff only mordenite occurs crystallising directly from devitrified glass shards. Clay minerals present are smectite and illite, and chlorite in highly altered volcaniclastic sediments. Interbedded mudstones sealed fluids into volcaniclastic sandstone and tuff horizons and diagenesis occurred in a closed hydrologic system. The original pore fluid, believed bicarbonate-rich, precipitated calcite cement in the absence of vitric debris. In volcaniclastic and vitric rocks devitrification of glass liberated alkalies and silica into pore fluids leading to crystallisation of zeolite. Conglomerates filling channels cut into other sediments were an open hydrologic system and analcime crystallised from Na-saturated fluids flowing through them. | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 03886298 | |||||
NII論文ID | ||||||
関連タイプ | isIdenticalTo | |||||
識別子タイプ | NAID | |||||
関連識別子 | 110000413352 | |||||
NII書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00103190 | |||||
フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |